According to the time-predictable model, after an earthquake, strain accumulates steadily as the shifting tectonic plates continuously grind together. Thus "if you know the size of the most recent earthquake and the rate of strain accumulation afterwards, you should be able to forecast the time that the next event will happen simply by dividing the strain released by the strain-accumulation rate," explains Jessica Murray, a geophysics graduate student at Stanford University. To test the theory, she and Paul Segall, also at Stanford, applied it to data collected from a town in central California known as Parkfield, which rests on the infamous San Andreas Fault (see image). Parkfield, it turns out, has suffered five quakes measuring magnitude 6 on the Richter scale at regular intervals since 1857, with the last one striking in 1966. "Parkfield is a good place to test the model because we have measurements of surface ground motion during the 1966 earthquake and of the strain that¿s been accumulating since," Murray observes. "It¿s also located in a fairly simple part of the San Andreas system because it¿s on the main strand of the fault and doesn¿t have other parallel faults running nearby."
Murray and Segall determined that the strain released in the 1966 quake had actually recovered by 1987. The earthquake that one would expect based on the time-predictability model has not come, however. "In fact, 15 years have gone by," Murray notes. "Our results show, with 95 percent confidence, that it should definitely have happened before now, and it hasn¿t, so that shows that the model doesn¿t work¿at least in this location." And if it doesn¿t work in a tectonically simple setting like Parkfield, she adds, it¿s even less likely to make accurate predictions in more complex locales, like the Bay Area or Los Angeles.